Earthquake nucleation and fault slip complexity in the lower crust of central Alaska
Earthquake nucleation and fault slip complexity in the lower crust of central Alaska
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London: Nature Publishing Group UK
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Language
English
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London: Nature Publishing Group UK
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Contents
Earthquakes start under conditions that are largely unknown. In laboratory analogue experiments and continuum models, earthquakes transition from slow-slipping, growing nucleation to fast-slipping rupture. In nature, earthquakes generally start abruptly, with no evidence for a nucleation process. Here we report evidence from a strike-slip fault zon...
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Earthquake nucleation and fault slip complexity in the lower crust of central Alaska
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TN_cdi_hal_primary_oai_HAL_hal_02019296v1
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_02019296v1
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ISSN
1752-0894
E-ISSN
1752-0908
DOI
10.1038/s41561-018-0144-2